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The geology of Russia, the world's largest country, which extends over much of northern Eurasia, consists of several stable cratons and sedimentary platforms bounded by orogenic (mountain) belts. European Russia is on the East European craton , at the heart of which is a complex of igneous and metamorphic rocks dating back to the Precambrian .
Trofimuk Institute of Petroleum-Gas Geology and Geophysics of the Siberian Branch of the RAS, IPGG SB RAS (Russian: Институт нефтегазовой геологии и геофизики имени А. А. Трофимука СО РАН, ИНГГ СО РАН) is a research institute in Novosibirsk, Russia. It was founded in 2005.
The research organization was established in 1957. [1] In 1960, the main scientific activity of the institute was associated with oil development in the West Siberian Lowland. [ 1 ]
[1] [2] The Gornaya Shoria megaliths, also known as the Surak-Kuilum megalithic complex and by other names, form the ridgecrests and summit of Mount Kuylyum (Kuilum, Kulyum)(Russian: Горна Куйлюм), 1,203 m (3,947 ft) in elevation. The base of this mountain is located 8 km away from the village of Orton (Russian: Ортон). Mount ...
The main activities of service: basic research and applied research in the field of seismology and geophysics, as well as conducting continuous seismic monitoring of the Russian Federation, tsunami warning in the Russian Far East, monitoring volcanic activity in Kamchatka and slow monitoring of geodynamic processes in the crust and ground deformation, carrying out continuous seismic monitoring ...
Southern Russia or the South of Russia (Russian: Юг России, IPA: [juk rɐˈsʲiɪ]) is a colloquial term for the southernmost geographic portion of European Russia. The term is generally used to refer to the region of Russia's Southern Federal District and North Caucasian Federal District .
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Geography of European Southern Russia. Subcategories. This category has the following 13 subcategories, out of 13 total. A. Geography of Adygea (3 C, 1 P)